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地下水埋深与“四水”转化参数关系探讨 总被引:1,自引:0,他引:1
阐述了“四水”转化的地表径流系数、降水入渗补给系数、降水入渗的土壤水资源系数和水资源系数随地下水埋深变化而变化的各自特点及各参数之间的相互关系,阐明了地下水埋深变化导致各参数变化以及各参数之间相互变化关系的内在原因。从“四水”转化的角度阐明了土壤水资源概念及其内涵。 相似文献
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大气水—地表水—土壤水—地下水相互转化关系的试验研究 总被引:4,自引:0,他引:4
本文重点研究了有作物条件下不同供水农田的“四水”相互转化,突出了有作物条件下降水入渗、潜水蒸发的差异性,土壤水在农业生态环境中的重要性,为水资源多目标开发,探索新路子。 相似文献
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基于对洛惠渠灌区农业水资源自然一人工复合循环转化系统分析,辨证地论述了人为水事活动对“四水”转化及其农业生态环境的影响,进而指出实行地表水与地下水的联合运用、强化农业水资源的地下蓄调是洛惠渠灌区农业水资源综合调节、合理配置的有效途径。 相似文献
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许志荣 《水文地质工程地质》1981,(4)
历史上黄淮海平原旱涝碱咸相随,长期影响农业的发展,积盐和脱盐、咸和淡、它们之间相互对立而又统一于一个“水”之上,要加快农业步伐,必须首先从“水”字着眼,综合治理旱涝碱咸,而水资源状况如何,又是综合治理的基础。黄淮海平原水资源状况究竟如何?看法很不一致。我认为黄淮海平原水资源是比较丰富的,开发利用潜力的很大。 相似文献
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关于土壤水资源评价方法的商榷 总被引:3,自引:0,他引:3
本文介绍了有关土壤水资源的一般概念,对目前采用的评价方法进行了修正,并根据“四水”转化关系,提出了由降雨转化成土壤水调节量的计算方法。 相似文献
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甘肃河西地区人类的生存发展对水资源的依赖性很高,且对水资源影响频繁,本地区"降水~地表水~土壤水~地下水"之间的水量转化关系复杂,难以直接观测到各种水的量及变化规律。由于观测资料缺乏,水资源转化规律及模型的研究一直是一个难题。选取观测资料(1982-2005年)相对完备且具有代表性的酒泉盆地,从盆地水资源系统转化机理和转化规律入手,利用水均衡的观点,提出酒泉盆地水资源转化关系模型,分析得出水资源使用状况,并对地下水的开采使用情况提出了建议。 相似文献
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地上水地下水联合运用实现灌区多目标综合治理 总被引:2,自引:0,他引:2
中国北方水资源短缺,实行地上水地下水联合运用是合理开发利用水资源与综合治理旱涝碱咸的基本途径。本文介绍地上水地下水联合运用,关键在于调控地下水理深在适宜的动态,以浅层地下水的地层空间作为调节“四水”(降水、土壤水、地下水、地上水)的地下水库,最大限度地把天然降雨转化为可利用的水资源,使地表径流充分拦蓄利用,增强防涝淋盐和淡化地下水质的作用,达到灌区多目标综合治理。 相似文献
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Alessandro Tarantino Andrew M. Ridley David G. Toll 《Geotechnical and Geological Engineering》2008,26(6):751-782
This paper presents a review of techniques for field measurement of suction, water content, and water hydraulic conductivity
(permeability). Main problems in the use of field tensiometers are addressed and hints on how to improve tensiometer performance
are given. Advantages and limitations of instruments for indirect measurement of suction including electrical conductivity
sensors, thermal conductivity sensors, dielectric permittivity sensors, filter paper, and psychrometer are discussed. Techniques
for water content measurement based on dielectric methods are then presented. These include time and amplitude domain reflectometry
and capacitance. Finally, a brief overview of methods for measurement of water permeability in the field is presented. 相似文献
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Natural granite and gabbro samples, with dimensions of the orderof 1 cm, were exposed up to 48 hours to water at a pressureof 2 kb and temperatures up to 1060 °C, in an internallyheated pressure vessel. Spatial and temporal nonequilibriummelt distributions were quantitatively studied in thin sectionsof the quenched samples. The main observations, in granite atabout 1020 °C, indicated that melting fronts were initiatedat grain boundaries exposed to water and advanced at initiallyhigh rates subject to rate limitation by water diffusion throughthe deepening melt. The melting slowed down sharply with a slightundersaturation due to exhaustion of free water in the inter-granularvoids. The experimental observations on melting rates and water diffusion,as a function of water concentration and temperature, are correlatedwith data derived from other studies. A new model is advancedfor water diffusion in granitic magma. It is demonstrated thatrate processes in silicate melts may be significantly acceleratedby water in differing patterns. Water diffusion in graniticmelt is rather insensitive to water concentration whereas meltingkinetics and fluidity are strongly enhanced by water but significantlydecoupled from each other, all in contradiction to standardkinetic theories. Melting kinetics is shown to be especiallycritical in physical experiments on melting rock, and some observationson electrical conductivity are accordingly re-interprete. 相似文献
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Philip E. LaMoreaux Ph.D. 《Environmental Geology》1990,16(3):169-169
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黔西林泉片区表层岩溶带发育特征及供水 总被引:1,自引:0,他引:1
贵州省黔西县林泉片区属于深切河谷斜坡地带,区内地下水位受乌江期隆升作用埋深大,不利于地下水的开发利用;且区内缺水人口分散分布于河谷斜坡地带,不利于集中供水。所以对区内表层岩溶带发育及表层带岩溶水分布特征的研究,是解决区内缺水问题的关键。 相似文献
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山西朔州市北邢家河饮用天然矿泉水 总被引:1,自引:0,他引:1
朔州市北邢家河村SB-2井,为第四系松散层孔隙承压水,井深7lm,水位埋深10.05m。动水位埋深17.8m,涌水量58.85m ̄3/h。经权威部门理化检测,省级评审确认该井水为低矿化度、锶、重碳酸钙·镁型饮用天然矿泉水,具良好的开发利用条件。 相似文献
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A variety of water supply sources are used in the rural Guatemalan Highlands. Formal municipal systems are rare, but villagers
frequently form local water committees that construct spring-based supply systems. Recent work has indicated that groundwater
may be a viable water supply source. The water quality from these two sources was characterized as well as water from other
common sources including surface water and precipitation collection systems. Typically, all of the water sources contained
unacceptable levels of coliform bacteria except for groundwater from a drilled well. Water monitoring indicated that not only
did the water contain coliforms at the actual sources, but the infrastructure used to transmit the water to points of use
may also be a source of coliforms. A cost comparison indicates that groundwater may be a cost-competitive, higher quality
alternative to traditional spring-fed water systems. 相似文献
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A. J. R. White 《Australian Journal of Earth Sciences》2013,60(4):551-555
Dehydration (vapour absent) partial melting reactions in the Earth's crust produce a hydrous granitic melt phase, new anhydrous minerals that are mostly pyroxenes, and new plagioclase more calcic than the initial plagioclase. These solid phases of the melt reaction are restite. If the restite is carried to high levels in the crust as a component of the magma, cooling and crystallisation to granite will result in back reactions in which the H2O in the melt phase is consumed and is not then available to form a hydrothermal solution. Even in magmas in which some restite has been removed there will be some back reaction and again less H2O. Only fractional crystallisation will enrich the H2O in the magma in sufficient amounts to form a substantial quantity of hydrothermal solution and possible mineralisation. 相似文献
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浙江省地处环太平洋火山带和中国东南沿海火山带,火山岩分布广泛。本文论述浙江省火山岩地区温泉、矿泉水的分布及其特征,分析火山岩岩性、岩石化学、构造性质及地貌因素对温泉、矿泉水形成的影响,提出火山岩地区温泉、矿泉水综合开发利用的意义,以及综合开发利用中应注意的问题。 相似文献